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Elemental composition and residual water content of seven thaliacean (salps a...
Ecosystem models often use wet weights to parameterise biota disregarding their water content. This may be especially erroneous for gelatinous plankton, such as salps and... -
Ground vegetation cover at 47 lake sites in Central and Eastern Yakutia, Sibe...
The vegetation surveys were carried out in four different study areas in the Sakha Republic, Russia: in the mountainous region of the Verkhoyansk Range within the Oymyakonsky... -
Ocean Sampling Day (OSD) 2014: AUTHORITY-RAW amplicon and metagenome sequenci...
Sequencing of amplicon and metagenome samples from the main OSD event, representing joint effort of marine sampling stations around the world. The OSD campaign aims to analyze... -
Major element compositions of Hole CM2B
This dataset has no description
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Major element compositions of Hole CM1A
Total carbon (wt.% oxides), hydrogen (wt.% oxides) and sulfur (wt.% oxides) compositions were measured by CHNS and inorganic carbon by coulometry on-board D/V Chikyu. Major... -
Gas contents of fluid inclusions in the Yaogangxian tungsten, South China
This dataset has no description
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XRF bulk rock data from serpentinites and ophicalcites of the northern Apenni...
This dataset has no description
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Benthic cover for Troux aux Biches and Flic en Flac lagoons, Mauritius
This dataset has no description
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Loss on ignition of the uppermost sediment record of Biển Hồ maar lake, Centr...
This dataset has no description
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(Tabel S5d) Plagioclase-hosted melt inclusions analyzed for their volatile co...
This dataset has no description
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(Tabel S5c) Clinopyroxene-hosted melt inclusions analyzed for their volatile ...
This dataset has no description
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(Tabel S8) Details of SIMS analyses of volatiles
Analyses indicated "BLK" in the sample name denote blank analyses on host crystals (without inclusions). -
Effect of salinity on burrowing behavior of soft shell clams Mya arenaria
Salinity changes in coastal zones is a frequent phenomena and coastal soft bottom organisms withstand these changes in a daily basis. This fluctuation in salinity can affect the... -
(Table 9, Page 43) Chemical composition of Mn nodules recovered during the GH...
The outer rind has been seperated from the foreign core for analysis and dessicated at 850°C.From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical... -
(Table 4) Geochemical fluxes at DSDP Hole 83-504B
Errors calculated from data in Tables 1-3 are given as ± g/100 cm**3 basalt at the 95% confidence level: SiO2: 10.96, TiO2: 0.53, A12O3: 5.76, Fe2O3: 0.42, FeO: 0.89, MnO: 0.41,... -
(Table 2) Percentage of fresh water in the surface water layer of the Arctic ...
This dataset has no description
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Average compositions of serpentine and fuchsite from hole BT1B, Oman Drilling...
The presented serpentine and fuchsite (Cr-muscovite) data were derived from representative carbonate-bearing serpentinite and listvenite samples from Hole BT1B, OmanDP. Electron... -
Israeli Mediterranean vermetid reef biodiversity monitoring data
Data presented are percent cover or count averages of 15 quadrats randomly placed along a 50 meter transect placed parallel to the shoreline at one of four intertidal zones at... -
Raman spectra of hydrous Mid-Ocean Ridge, Back-Arc Basalt and Ca alumino-sili...
Raman spectra of Mid-Ocean ridge basalts (MORBs), back-arc basalts (BABs) and Ca alumino-silicate glasses (eutectic quart-wollastonite-anorthite) were collected at the Research... -
(Table 1) Determined and theoretical chemical composition of thaumasite of OD...
Hole 841B was drilled in the forearc region of the Lau Basin at a water depth of 4810 m. The hole penetrated a roughly 500-m-thick series of Miocene volcanic sediments with a...